“…Physical Separations. The density fractionation of crushed coal in heavy liquids (chemically inert to coal constituents) is a very important procedure for the concentration and subsequent characterization of IM and MM in coal. ,,,,,,,,− For example, the coal fractions separated by heavy liquids with density <1.6, 1.6−2.9, and >2.9 g/cm 3 are normally the most useful because they are related, respectively, to the enrichment of OM, some rock-forming minerals and phases (quartz, feldspars, clay and mica minerals, calcite, magnesite, dolomite, ankerite, gypsum, volcanic glass), and heavy accessory minerals (As, Cu, Pb and Zn sulfides, Al, Cr, Fe and Ti oxides, zircon, garnet, Fe sulfates, barite, celestine, anglesite, witherite, strontianite, smithsonite, apatite, monazite, xenotime, scheelite) plus certain heavy Fe sulfides and carbonates (pyrite, marcasite, pyrrhotite, siderite). Naturally, in most cases these minerals are finely dispersed in coal and intimately associated with OM in particles and they are difficult to separate in heavier concentrates and commonly pass to lighter fractions (clay minerals, sulfates, carbonates, and occasionally sulfides).…”